Tag Archives: antarctica

With global climate change in effect the Arctic ice sheet has been losing area and has gone from 7.5 million km^2 in 1979 to 4 million km^2 in 2016 (Figure 1). The loss of ice coverage is detrimental to many species, but on the other hand opens up areas to new fishing grounds, oil and gas deposits, deep sea minerals, and shorter shipping routes that were previously inaccessible. While economically it is beneficial to exploit these now accessible resources, it is also necessary to designate Marine Protected Areas (MPAs) to preserve habitat and biodiversity.

Year round see ice cover for the periods of 1979-1984 and 2012-2016.

Geomorphic features such as seamounts, submarine canyons, hydrothermal vents, submarine plateaus, ridges, and escarpments serve as a proxy for benthic communities and ecological processes as they are often areas of high biodiversity and important to processes such as upwelling. Harris et al looked at the distribution of geomorphic features on the sea floor to assess their current level of protection within MPAs. They also aimed to see if these features were occurring within or outside of MPAs and identify ones that were once inaccessible due to year round sea ice.

To determine their area of study, Harris et al used the average minimum sea ice coverage from 1979-1983. They looked at the years 1979-1983 and 2012-2016 (the earliest and latest time periods) to see how much of the geomorphic features are now exposed. Twenty-nine categories of features were mapped using Shuttle Radar Topography Mapping (Shuttle Radar Topography) and MPA boundaries were taken from the IUCN and UNEP-WCMC database. The program ArcGIS was then used to compute areas.

On average, 31% of all previously year round covered features in the Arctic are now in open water in September. In 1979-1983, only 2.33% of areas below year round sea ice were in MPAs, and these were mostly areas on coastal and shelf habitats (Figure 2). This lack of diversity in features that are protected means there is high potential for them to be exploited now that year round ice no longer prevents access.

MPAs within the Arctic in relation to September sea ice cover in the periods 1979-1983 and 2012-2016.

As it stands, only 2.3% of the areas used in this study are in MPAs. While this seems to pose a problem, Canada, Denmark, Russia, Norway, and the USA have signed a “Declaration concerning the regulation of unregulated high seas fishing in the central Arctic Ocean” and a moratorium. Thereby, the areas beyond national jurisdiction have a degree of protection from fishing pressure at the current time.

Current MPAs mostly cover coastlines and inner shelf regions. Abyssal plains are not covered at all and there negligible protection for slope habitats. While the current MPAs do provide a small effect, they are not representative in the standard MPA design.

There are many geomorphic features that have been left exposed and all are fragile ecosystems. Basins collect sediment and anthropogenic contaminants, making them particularly susceptible to pollution from runoff and chemicals. Submarine canyons are considered biodiversity hot spots and prime fishing grounds, making them vulnerable to degradation. Only .2% of canyons are within existing MPAs and retreating sea ice now exposes 37% of their area. Submarine canyons face particular danger because they are associated with oil and gas deposits. Plateaus are mostly unexplored worldwide and thus need further examination and protection.

These underwater geomorphic regions are high in biodiversity but are finding themselves in peril with retreating sea ice. Many of these areas are likely under rapid ecological transition as the Arctic responds to global climate change. These ecosystems are highly unexplored and sensitive. They could be lucrative economically, but are also most likely highly important for conservation. MPAs will play a major role in protecting these areas.

Throughout history, both natural and man-made causes have resulted in long-lasting effects on the oceans. While most organic processes yield gradual change, the impact of human activity alters nature by prompting and accelerating otherwise irregular events (e.g. rapid ocean acidification, warming, habitat destruction), diminishing the oceans’ supply of pristine areas and ecosystems. A “pristine ecosystem” is defined as an area that has been either minimally affected or entirely untouched by human activity/influence. The depletion of these pristine areas impedes upon the ability to observe marine environments in their natural, undisturbed states. However, not all pristine marine habitats have been affected just yet.

A study conducted by a group of scientists based in Barcelona, Spain recently explored the pristine populations of deep-water corals on the Antarctic continental shelf. Thanks to geographical factors, the practically desolate waters of the Antarctic have provided protection to these gorgonian species from human influence and this study, as one of the first of its’ kind, has contributed to filling several gaps regarding the population characteristics of this species. While little was known about their distribution, abundance, and demographics, ROVs (remotely operated vehicles) have proven that gorgonians play an important role in the creating the geographical structure of many Antarctic continental shelfs by adding a three-dimensional aspect to their habitat. The purpose of this study was to learn about and understand the ecological role of these corals, which can be used in conservation efforts.

The results showed that coral populations in Antarctic benthic environments were not only booming, but that their distribution gradually differed between the Northern and Southern regions of the Weddell Sea. They thrive at depths of 250-350m and despite such extreme conditions, gorgonian density is similar to coral population values in temperate and tropical ocean floors. This discredits the widely accepted belief that species richness proportionately decreases with increasing latitude. Hydrodynamic conditions are also favorable for gorgonians at these depths by accumulating particle suspension in the near-bottom water layers. These strong currents are advantageous by providing a constant food supply and keeping reefs clear of sediment.

While gorgonian populations proved to be overwhelmingly healthy in the Antarctic, they are exposed to certain environmental threats that a tropical reef would never face. Due to their slow growth rate and reproduction type, gorgonians are especially vulnerable to iceberg scouring. Iceberg scouring events occur when icebergs drift into shallow areas and come into contact with/scrape the seafloor as it moves along. Additionally, anthropogenic activities such as bottom-trawling and by-catch fishing result in large habitat destruction for these species. The authors of this study hope to bring awareness to the abundance and health of gorgonians, which can at least begin to protect them from human-related threats.

A diagram portraying iceberg scouring, the process by which icebergs scrape the seafloor as it drifts through the ocean. Iceberg scouring events pose a threat to gorgonian species on the Antarctic continental shelf because of their slow growth rate, reproduction type, and inability to quickly recover. Flickr.

When one thinks of Antarctica, the first things that come to mind are frigid, icy weather and penguins. Therefore, it may come as a surprise to many that Antarctica is home to a variety of plant communities. Only 0.34 % of the Antarctic continent, and approximately 3% of the Antarctic Peninsula and offshore islands, is free of the snow and ice covering that transforms the remainder of the continent into a frozen wasteland. Only a small fraction of the ice-free land is able to support plant life: most of it is high latitude desert, rock faces protruding out of the ice sheets, and high altitude mountain ranges. This confines most visible terrestrial life to the coasts, predominantly along the Eastern coastline, the Antarctic Peninsula, and the Scotia Arc archipelagos.

Even the most diverse parts of Antarctica have relatively little botanical biodiversity compared to other ecosystems. The majority of Antarctic primary producers are cryptogams, seedless autotrophs that generally grow low to the ground, such as mosses, lichens, and liverworts. There are only two vascular plant species native to the continent. In addition to true plants, Antarctica is home to substantial microflora communities consisting of fungi, algae, and cyanobacteria. Vascular plants and bryophytes (nonvascular plants like mosses and liverworts) inhabit primarily coastal areas while inland and areas with high elevation are dominated by microfloral communities and lichens. These colonizable sites devoid of ice are few and far between, often separated by stretches of ocean or ice that can be hundreds of kilometers long. Isolation to this extent hinders the ability of plant species to colonize new land, restricting them to specific areas. This separation has prevented gene flow between distinct Antarctic plant communities, evolutionarily isolating them; in other words, these communities will continue to grow and adapt on their own, with the potential to eventually develop into distinct species. The regional disparities in terrestrial biodiversity make it very easy to divide the continent into specific biogeographic regions; 15 Antarctic Conservation Biogeographic Regions (ACBRs) have been identified to provide a formal structure upon which to develop a conservation plan for Antarctica and the organisms that inhabit it.

As human activity on Antarctica increases, it is becoming more apparent that an effective conservation strategy for the continent is necessary. Construction, overland transport, and continuing operation all threaten terrestrial organisms, especially those inhabiting coastlines, where most tourist and research practices are focused. Humans may also introduce invasive species, which could have detrimental effects on indigenous botanical biota. Plant communities are also facing destruction at the hands of fur seals, whose expanding range has increased the amount of vegetation they trample and damage in the Antarctic Peninsula. In addition to the threats affecting Antarctic plants in the immediate future, climate change has the potential to directly impact the continent’s flora.

Due to the scarcity and low diversity of Antarctic vegetation, these threats could cause severe damage, possibly wiping out entire communities or species in extreme scenarios. Recognizing the need for protection, the Protocol on Environmental Protection to the Antarctic Treaty instrumented Antarctic Specially Protected Areas (ASPAs) to maintain the diversity and health of representative Antarctic ecosystems. However, the effectiveness of this system is questionable; only 1.5 % of Antarctica’s ice-free terrain is under the jurisdiction of ASPAs and there are multiple regions with no ASPAs at all. 33 of the 72 established ASPAs specifically note protecting plant diversity as a management goal. Yet, these ASPAs include less than 0.5% of Antarctica’s ice-free ground and less than 16.1 km2 of vegetation cover. This is most likely only a small fraction of the continent’s botanical life, given a 2011 study that estimated 44.6 km2 of the northern Antarctic Peninsula alone has greater than 50% probability of vegetation presence. Another marked problem is that 96% of protected ice-free ground is within 2 ACBRs. This offers great protection for those habitats, but does not do an effective job of preserving diversity by concentration on only one or two ecosystems. It is blatantly apparent that Antarctica’s management strategies must be reworked in order to properly conserve both the health and diversity of its ecosystems.